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Assessment of the Quality of Soil and Groundwater of the Agricultural Area of Sidi Yahya Region, Morocco

机译:摩洛哥西迪亚赫亚地区农业区土壤和地下水的质量评估

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The Gharb plain is the largest agricultural area in Morocco. It is characterized by fertile soils and the availability of water either from surface or groundwater which allowed intensive agriculture. The aim of this research work is to study the impact of this land management on the quality of water and soil. The study was done for the irrigated perimeter of Sidi Yahya belonging to the province of Sidi Slimane, Gharb (Morocco). Depth of water table and water pH were measured in situ while water and soil samples were collected and brought to the laboratory for their physico-chemical analyses. Sampling of 33water wells and soil samples, from six different zones, was done between May and October 2018. Analysis of variance (ANOVA) was used to check if mean water and soil parameters differed between zones. The results showed that the minimal and maximal water table depth were 6 and 96 m, respectively. Also, slightly more than half of the wells (51.5%) were inadequate for irrigation since they were either highly or extremely saline. Furthermore, soils were poor to moderately poor in organic matter but very rich in potassium and the phosphorus content was highly variable. Based on the statistical analysis, it is clear that the six zones had significantly different means for CaCO_(3), pH, OM, and exchangeable sodium percentage. Soil degradation like pollution and salinization may occur in this region if poor quality water is used for irrigation and if land is mismanaged. This research work can be considered as a first step towards a program for monitoring the quality of soil and water for adapting the land management with the final objective of securing high productivity and sustainable use of soil and water resources.
机译:加尔布平原是摩洛哥最大的农业区。它的特点是肥沃的土壤和来自地表或地下水的水可利用性,可以进行集约化农业。这项研究工作的目的是研究土地管理对水和土壤质量的影响。这项研究是针对属于Gharb Sidi Slimane省(摩洛哥)的Sidi Yahya的灌溉边界进行的。在收集水和土壤样品并将其送至实验室进行理化分析的同时,现场测量了地下水位的深度和水的pH值。在2018年5月至2018年10月之间,对六个不同区域的33口水井和土壤样本进行了采样。方差分析(ANOVA)用于检查区域之间的平均水土参数是否有所不同。结果表明,最小和最大地下水位深度分别为6 m和96 m。同样,略多于一半的井(51.5%)由于盐分高或过高而无法灌溉。此外,土壤有机质差到中等差,但钾非常丰富,磷含量变化很大。根据统计分析,很明显,六个区域的CaCO_(3),pH,OM和可交换钠百分比的平均值均显着不同。如果使用劣质水灌溉和土地管理不当,该地区可能会发生土壤退化,例如污染和盐碱化。可以将这项研究工作视为朝着监测土壤和水质以适应土地管理的计划迈出的第一步,其最终目标是确保高生产力和水土资源的可持续利用。

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